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Lecture Outlines PowerPoint
Chapter 7
Earth Science, 12e
Tarbuck/Lutgens
Earth Science, Earth Science, 12e12e
Plate Tectonics: A Plate Tectonics: A Scientific Theory UnfoldsScientific Theory Unfolds
Chapter 7Chapter 7
Continental drift: an Continental drift: an idea before its time idea before its time
Alfred Wegener • First proposed hypothesis, 1915 • Published The Origin of Continents and
OceansContinental drift hypothesis• Supercontinent called Pangaea began
breaking apart about 200 million years ago • Continents “drifted” to present positions • Continents “broke” through the ocean crust
Pangaea approximately Pangaea approximately 200 million years ago200 million years ago
Figure 7.2
Continental drift: an Continental drift: an idea before its time idea before its time
Wegener’s continental drift hypothesis• Evidence used by Wegener
• Fit of South America and Africa • Fossils match across the seas• Rock types and structures match • Ancient climates
• Main objection to Wegener’s proposal was its inability to provide a mechanism
Similar mountain ranges Similar mountain ranges on different continentson different continents
Figure 7.7
Paleoclimatic Paleoclimatic evidence evidence
for for continentalcontinentaldriftdrift
Figure 7.8
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
More encompassing than continental drift Associated with Earth’s rigid outer shell • Called the lithosphere • Consists of several plates
• Plates are moving slowly • Largest plate is the Pacific plate • Plates are mostly beneath the ocean
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
Asthenosphere • Exists beneath the lithosphere • Hotter and weaker than lithosphere• Allows for motion of lithosphere Plate boundaries • All major interactions among plates occur
along their boundaries
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
Plate boundaries • Types of plate boundaries
• Divergent plate boundaries (constructive margins)
• Two plates move apart• Mantle material upwells to create new
seafloor • Ocean ridges and seafloor spreading
• Oceanic ridges develop along well-developed boundaries
• Along ridges, seafloor spreading creates new seafloor
Divergent boundaries are Divergent boundaries are located along oceanic ridgeslocated along oceanic ridges
Figure 7.11
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
Plate boundaries • Types of plate boundaries
• Divergent plate boundaries (constructive margins)
• Continental rifts form at spreading centers within a continent
• Convergent plate boundaries (destructive margins)
• Plates collide, an ocean trench forms, and lithosphere is subducted into the mantle
The East African rift The East African rift –– a a divergent boundary on landdivergent boundary on land
Figure 7.13
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
Plate boundaries • Types of plate boundaries
• Convergent plate boundaries (destructive margins)
• Oceanic–continental convergence• Denser oceanic slab sinks into the
asthenosphere • Pockets of magma develop and rise • Continental volcanic arc forms• Examples include the Andes, Cascades,
and the Sierra Nevadan system
An An oceanicoceanic––continentalcontinentalconvergent plate boundaryconvergent plate boundary
Figure 7.15 A
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
Plate boundaries • Types of plate boundaries
• Convergent plate boundaries (destructive margins)
• Oceanic–oceanic convergence• Two oceanic slabs converge and one
descends beneath the other • Often forms volcanoes on the ocean floor • Volcanic island arc forms as volcanoes
emerge from the sea • Examples include the Aleutian, Mariana,
and Tonga islands
An An oceanicoceanic––oceanicoceanicconvergent plate boundaryconvergent plate boundary
Figure 7.15 B
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
Plate boundaries • Types of plate boundaries
• Convergent plate boundaries (destructive margins)
• Continental–continental convergence• When subducting plates contain
continental material, two continents collide
• Can produce new mountain ranges such as the Himalayas
A A continentalcontinental––continentalcontinentalconvergent plate boundaryconvergent plate boundary
Figure 7.15 C
The collision of India and Asia The collision of India and Asia produced the Himalayas produced the Himalayas
Figure 7.16 A
The collision of India and The collision of India and Asia produced the Himalayas Asia produced the Himalayas
Figure 7.16 C
Plate tectonics: the Plate tectonics: the new paradigm new paradigm
Plate boundaries • Types of plate boundaries
• Transform fault boundaries• Plates slide past one another
• No new crust is created or destroyed • Transform faults
• Most join two segments of a mid-ocean ridge
• Aid the movement of oceanic crustal material
Testing the plate Testing the plate tectonics modeltectonics model
Evidence from ocean drilling• Some of the most convincing evidence
confirming seafloor spreading has come from drilling directly into ocean-floor sediment
• Age of deepest sediments• Thickness of ocean-floor sediments verifies
seafloor spreading
Testing the plate Testing the plate tectonics modeltectonics model
Hot spots and mantle plumes• Caused by rising plumes of mantle material• Volcanoes can form over them (Hawaiian
Island chain)• Mantle plumes
• Long-lived structures• Some originate at great depth, perhaps at the
mantle–core boundary
The Hawaiian Islands have The Hawaiian Islands have formed over a hot spotformed over a hot spot
Figure 7.21
Testing the plate Testing the plate tectonics modeltectonics model
Evidence for the plate tectonics model • Paleomagnetism
• Probably the most persuasive evidence • Ancient magnetism preserved in rocks • Paleomagnetic records show
• Polar wandering (evidence that continents moved)
• Earth’s magnetic field reversals• Recorded in rocks as they form at
oceanic ridges
Polar wandering paths for Polar wandering paths for Eurasia and North AmericaEurasia and North America
Figure 7.24 A
Paleomagnetic reversals Paleomagnetic reversals recorded by basalt flows recorded by basalt flows
Figure 7.27
Measuring plate motion Measuring plate motion Measuring plate motion• By using hot spot “tracks” like those of the
Hawaiian Island–Emperor Seamount chain• Using space-age technology to directly
measure the relative motion of plates • Very Long Baseline Interferometry (VLBI) • Global Positioning System (GPS)
Directions and rates Directions and rates of plate motionsof plate motions
Figure 7.28
What drives plate motion What drives plate motion
Driving mechanism of plate tectonics • No one model explains all facets of plate
tectonics • Earth’s heat is the driving force• Several models have been proposed
• Slab-pull and slab-push model • Descending oceanic crust pulls the plate • Elevated ridge system pushes the plate
Several mechanisms Several mechanisms contribute to plate motioncontribute to plate motion
Figure 7.29
What drives plate motion What drives plate motion Several models have been proposed• Plate–mantle convection
• Mantle plumes extend from mantle–coreboundary and cause convection within the mantle
• Models • Layering at 660 kilometers • Whole-mantle convection
Layering at 660 kmLayering at 660 km
Figure 7.30 A
WholeWhole--mantle convectionmantle convection
Figure 7.30 B
Plate tectonics into the future Plate tectonics into the future Present-day motions have been extrapolated into the future some 50 million years• Areas west of the San Andreas Fault slide
northward past the North American plate• Africa collides with Eurasia, closing the
Mediterranean and initiating mountain building
• Australia and new Guinea are on a collision course with Asia
A possible view of the world A possible view of the world 50 million years from now50 million years from now
Figure 7.31
End of Chapter 7End of Chapter 7